首页|基于不同量级日降雨的赣南湘水流域降雨侵蚀力时空变化特征分析

基于不同量级日降雨的赣南湘水流域降雨侵蚀力时空变化特征分析

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[目的]探明赣南湘水流域不同量级降雨侵蚀力时空变化特征,为该流域的土壤侵蚀防治和生态环境治理提供重要的科学依据.[方法]以赣南湘水流域为对象,采用章文波日降雨模型,通过对降雨侵蚀力的比较分析,筛选普通克里金插值(OK)、反距离加权插值(IDW)和径向基函数插值(RBF)中的最优插值方法,并对湘水流域降雨侵蚀力时空变化特征进行了分析.[结果]结果表明:①IDW比OK和RBF更适用于湘水流域.②1984-2021年湘水流域不同量级降雨侵蚀力、年降雨侵蚀力的空间分布差异均随量级的增大而增大,且二者总体均呈北部和南部偏高,中部偏低的趋势.③1984-2021年湘水流域年降雨、中雨、大雨和暴雨侵蚀力的变异系数(Cv)分别为0.26,0.15,0.25,0.47,均属于中等变异,且年际变化趋势均不显著.不同量级降雨侵蚀力的大小、所占年降雨侵蚀力的比例、年际变化速率随量级的增大而增大,且其震荡周期基本一致,均为3~4个震荡周期.[结论]赣南湘水流域北部是发生土壤侵蚀可能性较高的地区,因地制宜加强该地区水土保持措施将有助于湘水流域的土壤侵蚀防治.
Analysis of Spatiotemporal Variation Characteristics of Rainfall Erosivity in Xiangshui River Basin of Southern Jiangxi Province Based on Different Daily Rainfall
[Objective]The spatiotemporal variation characteristics of different magnitudes of rainfall erosivity in Xiangshui River basin of Southern Jiangxi Province were determined,in order to provide an important scientific basis for soil erosion prevention and ecological environmental management in the basin.[Methods]Taking Xiangshui River basin in Southern Jiangsu Province as the research object,the Zhang Wenbo daily rainfall model was used with comparative analysis of rainfall erosivity to select the optimal interpolation method among ordinary Kriging interpolation(OK),inverse distance weighted interpolation(IDW),and radial basis function interpolation(RBF).The spatiotemporal variation characteristics of rainfall erosivity was analyzed in Xiangshui River basin.[Results]① IDW was more suitable than OK and RBF in Xiangshui River basin.② The spatial distribution differences of rainfall erosivity and annual rainfall erosivity of different magnitudes in Xiangshui River basin from 1984 to 2021 increased with the increase of magnitude,and both showed an overall trend of higher values in the north and south,and lower values in the central region.③ The coefficients of variation of the erosion force of annual rainfall,moderate rain,heavy rain,and rainstorm in Xiangshui River basin from 1984 to 2021 were 0.26,0.15,0.25,and 0.47,respectively,all of which were classified as moderate variations,and the interannual variation trend was not significant.The magnitude of rainfall erosion force of different magnitudes,the proportion of annual rainfall erosion force,and the interannual change rate increased with the increase of magnitude.The oscillation cycles were basically the same,all of which were 3~4 oscillation cycles.[Conclusion]The northern part of the basin is a region with high possibility of soil erosion.Strengthening soil and water conservation measures in this region according to local conditions will help prevent and control soil erosion in the Xiangshui River basin.

Xiangshui River basinerosion of moderate rain,heavy rain,heavy rainrainfall erosion forceJiangxi Province

余敏琪、刘士余、盛菲、吴祎楠、刘长征

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江西农业大学国土资源与环境学院,江西南昌 330045

江西省鄱阳湖流域生态水利技术创新中心,江西南昌 330045

湘水流域 中雨、大雨、暴雨侵蚀力 降雨侵蚀力 江西省

国家自然科学基金项目江西省水利科学院开放研究基金项目

319603312023SKLS01

2024

水土保持通报
中国科学院水利部水土保持研究所 水利部水土保持监测中心

水土保持通报

CSTPCD北大核心
影响因子:0.658
ISSN:1000-288X
年,卷(期):2024.44(3)
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